MLchartDataset catalogue

Cyclostrophic flow

Term · Meteorology and atmospheric science · MLC-T-MET-004836

An idealized atmospheric flow where the Coriolis force is negligible compared to the pressure gradient force and the centrifugal force. This balance primarily occurs in small-scale, rapidly rotating vortices such as tornadoes and dust devils, where the radius of curvature is very small. In such flows, air parcels move in circular paths, with the pressure gradient force balanced by the centrifugal force.

Table 1. Record
IdentifierMLC-T-MET-004836
FieldMeteorology and atmospheric science
See alsoCyclostrophic wind
Record as JSON
{
  "id": "MLC-T-MET-004836",
  "term": "Cyclostrophic flow",
  "field": "Meteorology and atmospheric science",
  "definition": "An idealized atmospheric flow where the Coriolis force is negligible compared to the pressure gradient force and the centrifugal force. This balance primarily occurs in small-scale, rapidly rotating vortices such as tornadoes and dust devils, where the radius of curvature is very small. In such flows, air parcels move in circular paths, with the pressure gradient force balanced by the centrifugal force.",
  "see_also": [
    "cyclostrophic wind"
  ],
  "url": "https://mlchart.com/terminology/meteorology/cyclostrophic-flow/"
}

Record 2,422 of 10,816 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.